Seasonal Path of the Sun and Latitude Overview Details This lesson is a modification of what Dave Hess and I, Stan Skotnicki, use in our Earth Science classes at Cheektowaga Central High School. It is an extension of our lesson on Lesson Celestial Motions as we track the apparent path of the sun across the sky at different Arctic latitudes. Prior to this Lab activity they would have already created hemisphere models Less than a week of 42 North (mid-latitudes) and at the Equator 0. Download, Share, and Remix ✏ Working with Mike Loranty in Siberia during the summer of 2016 we experienced full High school and Up sunlight for 24 hours and has been a topic of conversation in class, which inspired me to extend our Apparent Path of the Sun lab to include latitudes at the arctic circle. Materials Objectives Explain how latitude affects the seasonal path of the Sun. During this lab activity, Clear plastic hemisphere model students will study the seasonal apparent path of the Sun above the Arctic Circle. Topics External protractor for model covered in this unit are coordinate location, insolation, celestial motions of Earth and the Dry erase markers – two different colors Sun, Seasons. Lesson Preparation Standards Prior to this lesson, students would have learned about the general motions between the Sun and Earth in relation to each other. The Apparent Path that the sun takes across the sky. There are also two other hemisphere model labs that would have been done before New York State this one, which are available on contact. The first model would have been created for 42 Physical Setting/Earth Science North and the other for the Equator at 0. Core Curriculum STANDARD 6 Interconnectedness: Common Procedure Themes MODELS: Complete procedures for the activity are listed on the worksheets of the Lab. Key Idea 2: Models are simplified representations of objects, structures, or Extension systems used in analysis, explanation, interpretation, or design. Additional hemisphere model labs have been created for 42 North and the Equator at 0. STANDARD 4 They can also be modified for any latitude desired. Key Idea 1: The Earth and celestial Resources phenomena can be described by principles of relative motion and perspective For data at any latitude at any interval: http://aa.usno.navy.mil/data/docs/AltAz.php Major Understandings: Can be modified for additional latitudes with data sets taken from 1.1a Most objects in the solar system are in http://aa.usno.navy.mil/data/docs/AltAz.php regular and predictable motion. • These motions explain such phenomena as the day, For an animation of the Apparent Path of the Sun at any Latitude: the year, seasons, phases of the moon, http://astro.unl.edu/naap/motion3/animations/sunmotions.swf eclipses, and tides 1.1c Earth’s coordinate system of latitude Material Resources - Clear plastic hemisphere model: and longitude, with the equator and prime https://www.wardsci.com/store/product/8889458/sun-tracking-hemisphere-kit meridian as reference lines, is based upon Earth’s rotation and our observation of the Assessment Sun and stars. This activity will be assessed as part of New York States minimum lab requirement for Regents credit. National Science Education Standards Author / Credits Content Standards, Grades 9-12 Content Standard A: Science As Inquiry Created by Stan Skotnicki ([email protected]) and Dave Hess from Cheektowaga Content Standard D: Earth and Space Central Schools Science NAME; PERIOD; DATE; LAB # SEASONAL PATH OF THE SUN AND LATITUDE Hemisphere Model #3 at the Arctic Circle 1 OBJECTIVE Explain how latitude affects the seasonal path of the Sun. I) Path of the Sun and Latitude. In the previous activity we observed that the Sun’s path across the sky varies with the seasons. As its path changes, so too does the position of sunrise and sunset, the altitude of the noon sun, and the duration of sunlight (length of daylight). In New York State, the Winter Solstice (on December 21), marks the time when the noon sun is lowest in the sky and the period of daylight is the shortest. The Summer Solstice (on June 21), is the day when the noon sun is highest in the sky and the duration of daylight is the greatest. Although the noon sun is highest on this date, the sun will never be directly overhead (zenith position) in New York State. In only place where the sun is ever in the zenith position (90o altitude), is in the tropics. The tropics is anywhere between 23.5oN and 23.5oS latitude. The path of the sun during the equinoxes lies between the paths for the solstices. The equinoxes (equal nights) are the only time when the sun rises due east and set due west. It is also the date when the entire Earth experiences 12 hours of sunlight, regardless of your location. Is the path of the Sun the same in New York as it is at the Arctic Circle, or at the equator? Does latitude (distance north or south from the equator) affect the path that the sun takes across the sky? Above the Arctic Circle, is there still 12 hours of daylight during the equinoxes? What will the duration of sunlight be like during the Solstices? By comparing three locations; NY (mid-latitudes), the Arctic Circle (66.5o), and the equator (0o) a conclusion can be made for how latitude affects the duration of sunlight for each season. 2 PROCEDURE Setting up the hemisphere model. 1) Turn to the last page of this lab. There should be a circle and the words “azimuth” on this page. Remove this page and tape it onto your piece of cardboard. 2) Label this piece of paper with your class period and all the members of your lab group. 3) Carefully place the hemisphere model on the circle. The hemisphere model should line up with the circle on the paper. 4) Use masking tape to fasten the hemisphere model to the cardboard. Place the tape at NE, SE, SW and NW. Marking the path of the Sun at 66.5° The Arctic Circle) 1) Find Data Table 1 (Azimuth and Altitude at a latitude of 90o The North Pole) Notice that there are only two available sets of data this time. - One set for both March and September 21 (the sun follows the same path on these days) – the “Spring Equinox” and the “Autumn Equinox” (First Day of Spring and the Frist Day of Autumn). - One set for June 21 – the first Day of Summer. 2) You will plot two lines on the hemisphere model – one for each set of data (each season). 3) Start with a green wet erase marker and plot the path of the sun for March/September 21. - For March/September 21the first set of data occurs at 6:00am; AZIMUTH 88o and ALTITUDE 1o - Azimuth values are listed along the circle. - Find the location for 0o (North) azimuth on the circle, move clockwise until you find 88o. - One member of the group lines up the external protractor with the azimuth value. This is done by holding the external protractor so that the 90o mark is at the top of the hemisphere model and the zero end points down towards the 88o reading for azimuth. - The second group member is responsible for placing a dot at the correct altitude on the hemisphere model. To do this read the value for altitude from the data table (in this case it is 0o), find where this number is on the external protractor, and use the green wet erase marker to place a dot at this location. 3 4) After all the points have been plotted, connect the points with a smooth curve. 5) Use the green marker to label this line; “March/September – Equinox”. Noon occurs when the Sun reaches its highest point in the sky (highest altitude). Place a small drawing of the sun over the point that represents the position of the noon sun. Write the word “noon” above this image. 6) Now do the same for June 21st data – use a red marker. Plot the points, label the line and identify the position of the noon sun. 4 Data Table 2 Azimuth and Altitude at a latitude at the Arctic Circle 66.5° Time of A.M. or December 21st March/September June 21st Day P.M. 21st Altitude Azimuth Altitude Azimuth Altitude Azimuth 12:00 A.M. - - - - 45 154 1:00 A.M. - - - - 47 174 2:00 A.M. - - - - 46 194 3:00 A.M. - - - - 44 213 4:00 A.M. - - - - 40 231 5:00 A.M. - - - - 35 247 6:00 A.M. - - 1 88 29 262 7:00 A.M. - - 6 102 23 276 8:00 A.M. - - 12 116 17 290 9:00 A.M. - - 17 131 12 302 10:00 A.M. - - 20 146 7 315 11:00 A.M. - - 23 162 4 329 12:00 P.M. - - 24 178 2 342 1:00 P.M. - - 23 194 1 356 2:00 P.M. - - 21 210 1 10 3:00 P.M. - - 17 225 2 23 4:00 P.M. - - 13 241 5 37 5:00 P.M. - - 7 256 9 50 6:00 P.M. - - 2 269 14 63 7:00 P.M. - - - - 20 76 8:00 P.M. - - - - 26 90 9:00 P.M. - - - - 32 104 10:00 P.M. - - - - 37 119 11:00 P.M. - - - - 42 136 5 Apparent Path of the Sun in Jamestown, NY 42°N – Mid-Latitudes Apparent Path of the Sun at the Equator 0° 6 Make Prediction on what the Path of the Sun might look like at the Arctic Circle 66.5° W N S E 7 Use the hemisphere model and/or data table to complete the following tables.